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Equinox transition at the magnetic equator in Africa: analysis of ESF ionograms

Abstract : We study equatorial night-time F layer behaviour from quarter-hourly ionograms at Korhogo/Ivory Coast (9.2° N, 5° W, dip lat. −2.4°) during local Spring March–April 1995, declining solar flux period, according to the magnetic activity. The height and thickness of the F-layer are found to vary intensely with time and from one day to the next. At time of the equinox transition, by the end of March, a net change of the nightly height-time variation is observed. The regime of a single height peak phase before 22 March changes to up to three main F-layer height phases after 30 March, each associated to a dominant mechanism. The first phase is identified to the post-sunset E×B pulse, the second phase associated to a change in the wind circulation phenomenon and the third one attributed to pre-sunrise phenomena. The influence of the magnetic activity is identified by the increase in the second peak amplitude. After the 21 April magnetic-equinox period, the height-time morphology becomes more irregular suggesting meridional wind abatement. The initiation, the growth and the maintenance of ESF are explored in relation to these nightly variations. The Rayleigh-Taylor instability is clearly identified as main precursor phenomenon. This is followed by the P-type (F-layer peak spread) structures, the whole with no specific dependence on the magnetic activity and on the F-layer phases, in contrast to further I and F-type (Inside and Frequency spread) ESFs. We discuss our results in the light of recent advanced experiments in Peru and the pacific.
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Submitted on : Thursday, December 17, 2015 - 6:03:44 PM
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B.J.-P. Adohi, P.M. Vila, Christine Amory-Mazaudier, Monique Petitdidier. Equinox transition at the magnetic equator in Africa: analysis of ESF ionograms. Annales Geophysicae, European Geosciences Union, 2008, 26 (7), pp.1777-1792. ⟨10.5194/angeo-26-1777-2008⟩. ⟨hal-00369442⟩



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